Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean
Identifieur interne : 001A83 ( Istex/Corpus ); précédent : 001A82; suivant : 001A84Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean
Auteurs : N. A. Bray ; S. E. Wijffels ; J. C. Chong ; M. Fieux ; S. Hautala ; G. Meyers ; W. M. L. MorawitzSource :
- Geophysical Research Letters [ 0094-8276 ] ; 1997-11-01.
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Abstract
Five hydrographic sections across the Indonesian throughflow from the World Ocean Circulation Experiment (WOCE) and the Java Australia Dynamic Experiment (JADE) are used to examine seasonal water mass and density distributions, including semiannual variation of the South Java Current. Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.
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DOI: 10.1029/97GL51793
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Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.</div></front></TEI><istex><corpusName>wiley</corpusName><keywords><teeft><json:string>woce</json:string><json:string>throughflow</json:string><json:string>salinity</json:string><json:string>intraseasonal</json:string><json:string>september</json:string><json:string>november</json:string><json:string>altimetric</json:string><json:string>bray</json:string><json:string>fieux</json:string><json:string>tions</json:string><json:string>indian ocean</json:string><json:string>april</json:string><json:string>wijffels</json:string><json:string>niiw</json:string><json:string>indonesian</json:string><json:string>indonesian throughflow</json:string><json:string>jade</json:string><json:string>csiro division</json:string><json:string>adcp data</json:string><json:string>noaa atlas nesdis</json:string><json:string>surfacedynamic height</json:string><json:string>altimeter data</json:string><json:string>eddy</json:string><json:string>meyers</json:string><json:string>cruise</json:string></teeft></keywords><author><json:item><name>N. 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Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.</abstract><qualityIndicators><score>4.986</score><pdfWordCount>1654</pdfWordCount><pdfCharCount>13537</pdfCharCount><pdfVersion>1.3</pdfVersion><pdfPageCount>4</pdfPageCount><pdfPageSize>579 x 817 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractWordCount>111</abstractWordCount><abstractCharCount>790</abstractCharCount><keywordCount>0</keywordCount></qualityIndicators><title>Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean</title><genre><json:string>article</json:string></genre><host><title>Geophysical Research Letters</title><language><json:string>unknown</json:string></language><doi><json:string>10.1002/(ISSN)1944-8007</json:string></doi><issn><json:string>0094-8276</json:string></issn><eissn><json:string>1944-8007</json:string></eissn><publisherId><json:string>GRL</json:string></publisherId><volume>24</volume><issue>21</issue><pages><first>2569</first><last>2572</last><total>4</total></pages><genre><json:string>journal</json:string></genre><subject><json:item><value>World Ocean Circulation Experiment: The Indian Ocean Expedition</value></json:item><json:item><value>Oceanography: General</value></json:item><json:item><value>Oceanography: General: General or miscellaneous</value></json:item><json:item><value>Oceanography: Physical</value></json:item><json:item><value>Oceanography: Physical: General or miscellaneous</value></json:item></subject></host><namedEntities><unitex><date><json:string>1992</json:string><json:string>1997</json:string><json:string>9500</json:string><json:string>1989</json:string><json:string>1995</json:string><json:string>1984</json:string><json:string>1989</json:string></date><geogName><json:string>Ocean South Equatorial Current</json:string><json:string>Sea Res</json:string><json:string>Altimetric sea</json:string><json:string>Ocean Wijffels</json:string></geogName><orgName><json:string>Division of Madonesian</json:string><json:string>Commonwealth Scientific</json:string><json:string>JADE</json:string><json:string>Industrial Research Organisation, Hobart, Tasmania, Australia</json:string><json:string>CalTech</json:string><json:string>Morawitz, Center for Coastal Studies</json:string><json:string>Change Research Program</json:string><json:string>Division of Oceanography</json:string><json:string>Deep Sea Research,Part I</json:string><json:string>Java Australia Dynamic Experiment</json:string><json:string>University of White</json:string><json:string>Research, Castray Esplanade, Hobart, TAS</json:string></orgName><orgName_funder></orgName_funder><orgName_provider></orgName_provider><persName><json:string>N. 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A.</forename><surname>Bray</surname></persName><affiliation>Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, California</affiliation></author><author xml:id="author-0001"><persName><forename type="first">S. E.</forename><surname>Wijffels</surname></persName><affiliation>Division of Marine Research, Commonwealth Scientific and Industrial Research Organisation, Hobart, Tasmania, Australia</affiliation></author><author xml:id="author-0002"><persName><forename type="first">J. 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Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.</p></abstract><textClass><classCode scheme="http://psi.agu.org/specialSection/WOCEEX1">World Ocean Circulation Experiment: The Indian Ocean Expedition</classCode><classCode scheme="http://psi.agu.org/taxonomy5/4200">Oceanography: General</classCode><classCode scheme="http://psi.agu.org/taxonomy5/4500">Oceanography: Physical</classCode></textClass><langUsage><language ident="en"></language></langUsage></profileDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/8DF70B68E0E00E44B9AC6BD6852934E1DACF404B/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Wiley, elements deleted: body"><istex:xmlDeclaration>version="1.0" encoding="UTF-8" standalone="yes"</istex:xmlDeclaration><istex:document><component type="serialArticle" version="2.0" xml:lang="en" xml:id="grl10767"><header><publicationMeta level="product"><doi>10.1002/(ISSN)1944-8007</doi><issn type="print">0094-8276</issn><issn type="electronic">1944-8007</issn><idGroup><id type="product" value="GRL"></id></idGroup><titleGroup><title type="main" xml:lang="en" sort="GEOPHYSICAL RESEARCH LETTERS">Geophysical Research Letters</title><title type="short">Geophys. 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A.</givenNames> <familyName>Bray</familyName></personName></creator><creator creatorRole="author" xml:id="grl10767-cr-0002" affiliationRef="#grl10767-aff-0002"><personName><givenNames>S. E.</givenNames> <familyName>Wijffels</familyName></personName></creator><creator creatorRole="author" xml:id="grl10767-cr-0003" affiliationRef="#grl10767-aff-0001"><personName><givenNames>J. C.</givenNames> <familyName>Chong</familyName></personName></creator><creator creatorRole="author" xml:id="grl10767-cr-0004" affiliationRef="#grl10767-aff-0003"><personName><givenNames>M.</givenNames> <familyName>Fieux</familyName></personName></creator><creator creatorRole="author" xml:id="grl10767-cr-0005" affiliationRef="#grl10767-aff-0004"><personName><givenNames>S.</givenNames> <familyName>Hautala</familyName></personName></creator><creator creatorRole="author" xml:id="grl10767-cr-0006" affiliationRef="#grl10767-aff-0002"><personName><givenNames>G.</givenNames> <familyName>Meyers</familyName></personName></creator><creator creatorRole="author" xml:id="grl10767-cr-0007" affiliationRef="#grl10767-aff-0001"><personName><givenNames>W. M. L.</givenNames> <familyName>Morawitz</familyName></personName></creator></creators><affiliationGroup><affiliation type="organization" xml:id="grl10767-aff-0001"><unparsedAffiliation>Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, California</unparsedAffiliation></affiliation><affiliation type="organization" xml:id="grl10767-aff-0002"><unparsedAffiliation>Division of Marine Research, Commonwealth Scientific and Industrial Research Organisation, Hobart, Tasmania, Australia</unparsedAffiliation></affiliation><affiliation type="organization" xml:id="grl10767-aff-0003"><unparsedAffiliation>Laboratoire d'Oceanographie Dynamique et de Climatogie, CNRS/ORSTOM/UPCM, Paris, France</unparsedAffiliation></affiliation><affiliation type="organization" xml:id="grl10767-aff-0004"><unparsedAffiliation>School of Oceanography, University of Washington, Seattle</unparsedAffiliation></affiliation></affiliationGroup><abstractGroup><abstract type="main"><p xml:id="grl10767-para-0001">Five hydrographic sections across the Indonesian throughflow from the World Ocean Circulation Experiment (WOCE) and the Java Australia Dynamic Experiment (JADE) are used to examine seasonal water mass and density distributions, including semiannual variation of the South Java Current. Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Characteristics of the Indo‐Pacific Throughflow in the eastern Indian Ocean</title></titleInfo><name type="personal"><namePart type="given">N. A.</namePart><namePart type="family">Bray</namePart><affiliation>Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, California</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">S. E.</namePart><namePart type="family">Wijffels</namePart><affiliation>Division of Marine Research, Commonwealth Scientific and Industrial Research Organisation, Hobart, Tasmania, Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">J. C.</namePart><namePart type="family">Chong</namePart><affiliation>Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, California</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Fieux</namePart><affiliation>Laboratoire d'Oceanographie Dynamique et de Climatogie, CNRS/ORSTOM/UPCM, Paris, France</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">S.</namePart><namePart type="family">Hautala</namePart><affiliation>School of Oceanography, University of Washington, Seattle</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">G.</namePart><namePart type="family">Meyers</namePart><affiliation>Division of Marine Research, Commonwealth Scientific and Industrial Research Organisation, Hobart, Tasmania, Australia</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">W. M. L.</namePart><namePart type="family">Morawitz</namePart><affiliation>Center for Coastal Studies, Scripps Institution of Oceanography, La Jolla, California</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article" authority="ISTEX" authorityURI="https://content-type.data.istex.fr" valueURI="https://content-type.data.istex.fr/ark:/67375/XTP-6N5SZHKN-D">article</genre><originInfo><publisher>Blackwell Publishing Ltd</publisher><dateIssued encoding="w3cdtf">1997-11-01</dateIssued><dateCaptured encoding="w3cdtf">1997-03-05</dateCaptured><dateValid encoding="w3cdtf">1997-05-19</dateValid><edition>.</edition><copyrightDate encoding="w3cdtf">1997</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><abstract>Five hydrographic sections across the Indonesian throughflow from the World Ocean Circulation Experiment (WOCE) and the Java Australia Dynamic Experiment (JADE) are used to examine seasonal water mass and density distributions, including semiannual variation of the South Java Current. Altimetric sea surface height variations match dynamic height along each WOCE cruise track remarkably well. They also reveal energetic eddies and meanders of the current system south of Java with intraseasonal (60‐day) changes in surface dynamic height comparable in magnitude to seasonal and interannual variations. Through the formation of discrete eddies and meanders of the large‐scale zonal flows, intraseasonal fluctuations account for much of the variation in water mass structure between cruises.</abstract><relatedItem type="host"><titleInfo><title>Geophysical Research Letters</title></titleInfo><titleInfo type="abbreviated"><title>Geophys. Res. Lett.</title></titleInfo><genre type="journal" authority="ISTEX" authorityURI="https://publication-type.data.istex.fr" valueURI="https://publication-type.data.istex.fr/ark:/67375/JMC-0GLKJH51-B">journal</genre><subject><genre>index-terms</genre><topic authorityURI="http://psi.agu.org/specialSection/WOCEEX1">World Ocean Circulation Experiment: The Indian Ocean Expedition</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4200">Oceanography: General</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4299">Oceanography: General: General or miscellaneous</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4500">Oceanography: Physical</topic><topic authorityURI="http://psi.agu.org/taxonomy5/4599">Oceanography: Physical: General or miscellaneous</topic></subject><identifier type="ISSN">0094-8276</identifier><identifier type="eISSN">1944-8007</identifier><identifier type="DOI">10.1002/(ISSN)1944-8007</identifier><identifier type="PublisherID">GRL</identifier><part><date>1997</date><detail type="volume"><caption>vol.</caption><number>24</number></detail><detail type="issue"><caption>no.</caption><number>21</number></detail><extent unit="pages"><start>2569</start><end>2572</end><total>4</total></extent></part></relatedItem><identifier type="istex">8DF70B68E0E00E44B9AC6BD6852934E1DACF404B</identifier><identifier type="ark">ark:/67375/WNG-HGQTJ9X8-5</identifier><identifier type="DOI">10.1029/97GL51793</identifier><identifier type="ArticleID">97GL51793</identifier><accessCondition type="use and reproduction" contentType="copyright">Copyright 1997 by the American Geophysical Union.</accessCondition><recordInfo><recordContentSource authority="ISTEX" authorityURI="https://loaded-corpus.data.istex.fr" valueURI="https://loaded-corpus.data.istex.fr/ark:/67375/XBH-L0C46X92-X">wiley</recordContentSource></recordInfo></mods><json:item><extension>json</extension><original>false</original><mimetype>application/json</mimetype><uri>https://api.istex.fr/document/8DF70B68E0E00E44B9AC6BD6852934E1DACF404B/metadata/json</uri></json:item></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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